{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1363670321177774720.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2004gl020884"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004GL020884"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004GL020884"}}],"dc:title":[{"@value":"Decadal weakening of the shallow overturning circulation in the South Indian Ocean"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Satellite observations reveal a substantial weakening of the southeasterly trade wind over the South Indian Ocean during 1992–2000 and a resultant slowdown of the shallow meridional overturning circulation in this Ocean. The estimated rate of the slowdown of this circulation, 6.8 ± 1.4 × 10<jats:sup>6</jats:sup> m<jats:sup>3</jats:sup>/s over the 9‐year period, is nearly 70% of the mean strength of this circulation. Such a change has important implications to upper‐ocean heat content and decadal climate variability of the Indian Ocean, as well as to the ecosystem and air‐sea exchange of CO<jats:sub>2</jats:sub> in the region.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670321177774720","@type":"Researcher","foaf:name":[{"@value":"Tong Lee"}],"jpcoar:affiliationName":[{"@value":"Jet Propulsion Laboratory California Institute of Technology  Pasadena California USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2004-09","prism:volume":"31","prism:number":"18","prism:startingPage":"L18305"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004GL020884"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004GL020884"}],"createdAt":"2004-09-24","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360022307172480768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reviews and syntheses: Physical and biogeochemical processes associated with upwelling in the Indian Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186513125248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mean Subsurface Upwelling Induced by Intraseasonal Variability over the Equatorial Indian Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092736818560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variability in Meridional Transport of the Subtropical Circulation in the South Indian Ocean for the Period From 2006 to 2017"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092737372032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interannual Variability in Sea Surface Height at Southern Midlatitudes of the Indian Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849943103658624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mechanisms of Long‐Term Variability and Recent Trend of Salinity Along 137°E"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892096587136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"What did determine the warming trend in the Indonesian sea?"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2004gl020884"},{"@type":"CROSSREF","@value":"10.1175/jpo-d-20-0279.1_references_DOI_EMMuKymTDf0kgjYyGpJQblSIeCg"},{"@type":"CROSSREF","@value":"10.1029/2019jc015874_references_DOI_EMMuKymTDf0kgjYyGpJQblSIeCg"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00334-2_references_DOI_EMMuKymTDf0kgjYyGpJQblSIeCg"},{"@type":"CROSSREF","@value":"10.1029/2019jc015290_references_DOI_EMMuKymTDf0kgjYyGpJQblSIeCg"},{"@type":"CROSSREF","@value":"10.1175/jpo-d-16-0257.1_references_DOI_EMMuKymTDf0kgjYyGpJQblSIeCg"},{"@type":"CROSSREF","@value":"10.5194/bg-18-5967-2021_references_DOI_EMMuKymTDf0kgjYyGpJQblSIeCg"}]}